[U-11] 第四紀および人新世の気候変動

[U11-P20] Glacial–interglacial CO₂ dynamics over the last 800 kyr revealed by multi-proxy geochemical analyses of planktic foraminifera from the South China Sea

*Yi-Ning Chen¹, Kuo-Fang Huang¹ (1. Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan)

キーワード：Glacial-interglacial cycles, CO2 dynamics, Ocean carbonate system, Boron isotopes, Foraminiferal shell chemistryForaminiferal shell chemistry, South China Sea